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Precipitation regime changes in High Mountain Asia driven by cleaner air

High Mountain Asia (HMA) has experienced a spatial imbalance in water resources in recent decades, partly because of a dipolar pattern of precipitation changes known as South Drying–North Wetting1. These changes can be influenced by both human activities and internal climate variability2,3. Although climate projections indicate a future widespread wetting trend over HMA1,4, the timing and mechanism of the transition from a dipolar to a monopolar pattern remain unknown. Here we demonstrate that the observed dipolar precipitation change in HMA during summer is primarily driven by westerly- and monsoon-associated precipitation patterns. The weakening of the Asian westerly jet, caused by the uneven emission of anthropogenic aerosols, favoured a dipolar precipitation trend from 1951 to 2020. Moreover, the phase transition of the Interdecadal Pacific Oscillation induces an out-of-phase precipitation change between the core region of the South Asian monsoon and southeastern HMA. Under m ....

Tibetan Plateau , China General , United States , United Kingdom , Charles Grifin , Us Geological Survey , Us Geological , Earth Environ , High Mountain Asia , Scientific Assessment , Third Pole Environment , United Nations Environment Programme , Hindu Kush Karakoram Himalaya , Change Res , Climate Change , Indian Region , Springer Singapore , Interdecadal Pacific Oscillation , North American , Physical Science Basis , Third Pole , Arctic Pole , Global Multi Resolution Terrain Elevation Data , Survey Open File Report , Global Precipitation Measurement , High Asia Refined ,